Variation in the structure of the surface layer of a heterogeneous solid (gneiss) on a shear
- Авторы: Vettegren’ V.I.1, Ponomarev A.V.2, Arora K.3, Mamalimov R.I.1, Shcherbakov I.P.1, Patonin A.V.4
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Учреждения:
- Ioffe Institute
- Schmidt Institute of Physics of the Earth
- CSIR National Geophysical Research Institute
- Borok Geophysical Observatory, Schmidt Institute of Physics of the Earth
- Выпуск: Том 59, № 7 (2017)
- Страницы: 1345-1348
- Раздел: Mechanical Properties, Physics of Strength, and Plasticity
- URL: https://journal-vniispk.ru/1063-7834/article/view/200488
- DOI: https://doi.org/10.1134/S1063783417070319
- ID: 200488
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Аннотация
The structure of surface layers with a thickness of ~1 μm formed at destruction of gneiss is studied by means of photoluminescent and infrared spectroscopy. It is found that, in this layer, feldspar (plagioclase and microcline) crystals are completely destroyed and replaced by montmorillonite.
Об авторах
V. Vettegren’
Ioffe Institute
Автор, ответственный за переписку.
Email: Victor.Vettegren@mail.ioffe.ru
Россия, St. Petersburg, 194021
A. Ponomarev
Schmidt Institute of Physics of the Earth
Email: Victor.Vettegren@mail.ioffe.ru
Россия, Moscow, 123242
K. Arora
CSIR National Geophysical Research Institute
Email: Victor.Vettegren@mail.ioffe.ru
Индия, Hyderabad, Telangana, 500007
R. Mamalimov
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
Россия, St. Petersburg, 194021
I. Shcherbakov
Ioffe Institute
Email: Victor.Vettegren@mail.ioffe.ru
Россия, St. Petersburg, 194021
A. Patonin
Borok Geophysical Observatory, Schmidt Institute of Physics of the Earth
Email: Victor.Vettegren@mail.ioffe.ru
Россия, Borok, Yaroslavl oblast, 152742
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